For years, scientists have studied trees to learn about yearly rainfall, temperature and climate over time. Now, a University of Arizona researcher is diving a little deeper to gather new climate data from an unexpected sea creature β a clam called a geoduck.
Funded by a three-year, $480,000 National Science Foundation grant, Bryan Black, an associate professor at the UAβs Laboratory of Tree-Ring Research, is using geoduck shells from the northeast Pacific Ocean to create a chronological history of climate in these waters. Geoduck, pronounced βgooey duck,β are a species of large edible saltwater clam.
Just like the rings that trees develop every year, clams also have climate information embedded within their shells. Each striation, or ridge, on the shell of a geoduck represents the passing of a year, and it contains clues about oceanic climate.
βIt turns out that clams form annual growth increments, or rings, just like trees do. And you can see these on the outside of many shells, including clams,β Black said. βSo, what we can do is cut through the middle of the shell and very carefully polish and prepare that surface to clearly reveal those growth increments.β
Geoducks can live to be about 180 years old, but their shells can survive in the water for an additional 2,000 years, according to radiocarbon data.
βWe can measure those growth increment widths to tell us something about the climate those clams experienced,β Black said. βThe width of each increment, or ring, in these clams is very strongly related to the temperature of the water temperature that they experienced that year.β
Climate Trends
For this project, Black hired a team of professional divers, who commercially fish for geoduck, to collect hundreds of shells and deliver them to his lab.
Once received, Black and his team slice the shells, cast them in epoxy, polish the surface of the epoxy, and measure the width of each striation. Then, through a process called crossdating, they establish the exact calendar year each striation was formed.
βCrossdating is the foundation of dendrochronology,β Black said. βAs climate varies from year to year, it induces a synchronous growth pattern or βbar codeβ among all individuals of a given species and site. By matching those βbar codesβ among shells, we can determine exactly when each individual lived and extend our record back in time.β
Using these techniques, Black and his team have successfully recorded a year-by-year history of the Pacific Oceanβs climate dating back to 1728.
In the Pacific North, there is a pattern of flipping between cool periods and warm periods every 20 to 30 years. According to Black, geoducks are very consistent in picking up these climate shifts, which is important because that flip-flopping between warm and cool periods is difficult to capture using trees alone.
βWhenever the North Pacific slips between one of these 20- or 30-year warm phases to a cool phase, it can profoundly rearrange the marine ecosystems and their functioning, with major impacts on fisheries, he said. βThis flip-flopping also strongly influences fire and drought, snowpack and river discharge in western North America, but we really donβt know how itβs behaved in the past, which is the goal of this research.β
With the data theyβve collected so far, Black said theyβve noticed strong warming trends, especially since the 1920s. Black hopes that as they continue to collect data, theyβll begin to understand this warming trend through a much longer-term context.
For postdoctoral researcher David Reynolds, this project is producing data that will have real world, global implications.
βOur understanding of how the oceans interact with the global climate is really not that great. Our modern observations really only go back about 50 years,β Reynolds said. βThis type of project where weβre looking at shells from the North Pacific really allows us to tackle those really big-picture, important questions. When we can integrate these data with numeric climate models, we can then help policymakers really understand how the climate is going to change in the future and what the uncertainties are around that.β
Inside Blackβs lab, Reynolds works with Ph.D. student David Edge and undergraduate Christine Outridge to process the clams, take images and analyze the data using a computer program that they developed.
Next Steps
The team hopes to be able to develop a 1,000-year chronology using climate information from geoducks.
As a researcher in the UAβs Tree Ring Lab, Black also hopes to combine this data with the chronologies of trees, which date as far back as 10,000 years.
βWe can relate this long geoduck chronology to trees to see if trees provide us some complimentary information about climate in the past and how the ocean and the atmosphere are linked,β he said.
Black also has colleagues who are working to develop chronologies from clams in the North Atlantic and is hoping to be able to compare data between two oceans to understand how climate has affected them differently over long periods of time.
βWe can get histories that span most of the past century, and that tells us a lot,β Black said. βWith these long chronologies, we can establish robust relationships between the biology and the climate.β